DIOPSIDE
, an important member of the See also:pyroxene See also:group of See also:rock-forming minerals
.
It is a See also:calcium-See also:magnesium metasilicate, CaMg (SiO3)2, and crystallizes in the See also:monoclinic See also:system
.
Usually some See also:iron is See also:present replacing magnesium, and when this pre-dominates there is a passage to hedenbergite, CaFe(SiO3)2, a closely allied variety of monoclinic pyroxene
.
These are distinguished from See also:augite by containing little or no See also:aluminium
.
Diopside is colourless, See also:- WHITE
- WHITE, ANDREW DICKSON (1832– )
- WHITE, GILBERT (1720–1793)
- WHITE, HENRY KIRKE (1785-1806)
- WHITE, HUGH LAWSON (1773-1840)
- WHITE, JOSEPH BLANCO (1775-1841)
- WHITE, RICHARD GRANT (1822-1885)
- WHITE, ROBERT (1645-1704)
- WHITE, SIR GEORGE STUART (1835– )
- WHITE, SIR THOMAS (1492-1567)
- WHITE, SIR WILLIAM ARTHUR (1824--1891)
- WHITE, SIR WILLIAM HENRY (1845– )
- WHITE, THOMAS (1628-1698)
- WHITE, THOMAS (c. 1550-1624)
white, See also:pale See also:green to dark green or nearly See also:black in See also:colour, the See also:depth of the colour depending on the amount of iron present
.
The specific gravity and See also:optical constants also vary with the chemical See also:composition; the sp. gr. of diopside is 3.2, increasing to 3.6 in hedenbergite, and the See also:angle of optical extinction in the See also:plane of symmetry varies between 38° and 47° in the two extremes of the See also:series, Crystals are usually prismatic in See also:habit with a rectangular See also:cross-See also:section as shown in the figure: the angle between the See also:prism faces m, parallel to which there are perfect cleavages, is 92° 50'
.
Several varieties, depending on See also:differences in structure and
chemical composition, have been distinguished, viz. coccolite (from KoKKOS, a See also:grain), a granular variety; salite or sahlite, from See also:Sala in See also:Sweden; malacolite; See also:diallage; violane, a lamellar variety of a dark See also:violet-See also:blue colour; chrome-diopside, a See also:bright green variety containing a small amount of See also:chromium; and many others
.
Belonging to the same series with diopside and hedenbergite is a See also:manganese pyroxene, known as schefierite, which has the composition (Ca, Mg) (Fe, Mn) (SiO3)2
.
Diopside is the characteristic pyroxene of metamorphic rocks, occurring especially in crystalline limestones, and often in association with See also:garnet and See also:epidote
.
It is also an essential constituent of some
pyroxene-granites, diorites and a few other igneous rocks, but the characteristic pyroxene of this class of rocks is augite
.
See also:Fine transparent crystals of a pale green colour occur, with crystals of yellowish-red garnet (hessonite) and See also:chlorite, in See also:veins traversing See also:serpentine in the See also:Ala valley near See also:Turin in See also:Piedmont: a crystal of this variety (" alalite ") is represented in the accompanying figure
.
These, as well as the See also:long, transparent, See also:bottle-green crystals from the Zillerthal in the Tyrol, have occasionally been cut as See also:gem-stones
.
See also:Good crystals have been found also at Achmatovsk near See also:Zlatoust in the Urals, Traversella near See also:Ivrea in Piedmont (" traversellite "), Nordmark in Sweden, See also:Monroe in New See also:York, See also:Burgess in See also:Lanark See also:county, See also:Ontario, and several other places: at Nordmark the large, rectangular black crystals occur with See also:magnetite in the iron mines
.
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.
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.
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